kaolinite and goethite

Biochar when applied into soil, together with soil clay minerals, may provide habitats for soil microbes and shift soil microbial community structure. Although several mechanisms have been proposed to explain the effects of biochar on microbial community, the impact of biochar on quorum sensing (QS) and QS-regulated behavior is poorly understood. In this study, we compared the effects of biochar and three common soil minerals (i.e., montmorillonite, kaolinite, and goethite) on QS and biofilm formation. Pseudomonas aeruginosa PAO1 with complete QS systems was selected as a model organism. Our results showed that biochar and goethite effectively promoted microbial QS and biofilm formation, while montmorillonite and kaolinite posed no significant effect. Live/Dead staining, SEM and density-dependent QS activity indicated that biochar was beneficial to cell viability maintenance and cell aggregations, which improved the efficiency of intercellular communications through QS. QS mutant strain experiments confirmed that biochar enhanced PAO1 biofilm formation by promoting QS. Goethite promoted biofilm formation with a different mechanism that cell debris induced by iron ions and positive charge on goethite surface provided raw materials for bacterial biofilm formation. Our findings provide evidence that the presence of biochar can enhance QS and biofilm formation through a feedforward loop of the QS system. This contributes to better understand biochar-mediated microbial cell to cell communications through QS.

Topics: Bentonite; Biofilms; Kaolin; Minerals; Pseudomonas aeruginosa; Quorum Sensing; Soil

Widespread antibiotic resistance genes (ARGs) have emerged as a focus of attention for public health. Transformation is essential for ARGs dissemination in soils and associated environments; however, the mechanisms of how soil components contribute to the transformation of ARGs remain elusive. Here we demonstrate that three representative mineral-humic acid (HA) composites exert contrasting influence on the transformation of plasmid-borne ARGs in

Topics: Adsorption; Anti-Bacterial Agents; Bentonite; Drug Resistance, Microbial; Humic Substances; Kaolin; Minerals; Soil

Persulfate (PS)-based in situ chemical oxidation (ISCO) has been widely used for pollutant remediation in soil and groundwater. However, the underlying mechanism of interactions between mineral and PS was not fully explored. In this study, several soil model minerals including goethite, hematite, magnetite, pyrolusite, kaolin, montmorillonite, and nontronite were selected to investigate their potential effects on PS decomposition and free radical evolution. It was found the decomposition efficiency of PS by these minerals varied significantly, and both the radical and non-radical decomposition processes were included. Pyrolusite has the highest reactivity for PS decomposition. However, PS decomposition is prone to form SO

Topics: Bentonite; Environmental Pollutants; Ferrosoferric Oxide; Kaolin; Minerals; Oxidation-Reduction; Phenols; Soil; Sulfates; Water Pollutants, Chemical

This study investigated the transport behavior of polystyrene microplastics (MPs) in saturated quartz sand and goethite-coated sand in the presence of coexisting kaolinite colloids. Column experiments were conducted under a wide range of solution chemistry conditions, including pH levels of 6.0, 7.0, and 9.0, as well as background Na

Topics: Colloids; Kaolin; Microplastics; Plastics; Polystyrenes; Porosity; Quartz; Sand; Silicon Dioxide

The current study investigated the use of VNIR-SWIR (visible/near infrared to short-wavelength infrared: 400-2500 nm) spectroscopy for predicting trace metals in overbank sediments collected in the study site. Here, we (i) derived spectral absorption feature parameters (SAFPs) from measured ground spectra for correlation with trace metal (Pb, Cd, As, and Cu) contents in overbank sediments, (ii) built univariate regression models to predict trace metal concentrations using the SAFPs, and (iii) evaluated the predictive capacities of the regression models. The derived SAFPs associated with goethite in overbank sediments were Depth433

Topics: Cadmium; Coal; Environmental Monitoring; Kaolin; Lead; Rivers; Spectrum Analysis; Trace Elements

Persulfate activation technology based on sulfate radicals is currently a hot spot in the field of environmental governance. In our work, α-FeOOH was successful in situ loaded on kaolinite surface through a simple one-step hydrothermal process. The prepared composites were systematically characterized, and the relationship between the structural properties and peroxymonosulfate activation properties was explored. Interestingly, compared to bare α-FeOOH, the introduction of kaolinite in composite induced the transformation of α-FeOOH crystal and affected the morphology, where uniformly dispersed nanoparticles rather than rod-like agglomerated crystals appeared. The received FeOOH/kaolinite composite exhibited admirable adsorption and degradation of ciprofloxacin performance with the removal efficiency of 86.1%, and the degradation rate constant was up to 5.2 times higher than that of bare α-FeOOH. In addition, the main active species in the catalytic oxidation system are surface-bound SO

Topics: Conservation of Natural Resources; Environmental Policy; Iron Compounds; Kaolin; Minerals; Peroxides; Water Pollutants, Chemical

The viable and degradation potential of the strains which adhered to soil minerals are essential for eliminating organic pollutants from soil. Herein, the interaction (growth, biofilm formation and survive) of Arthrobacter sp. DNS10, an atrazine degrading strain, with three kinds of typical soil minerals, such as montmorillonite, kaolinite and goethite, as well as the atrazine degradation gene (trzN) expression of the strain in the minerals system were studied. The results showed that montmorillonite had significant promotion effect on the growth of strain DNS10, followed by kaolinite, but goethite significantly inhibited the growth of strain DNS10. In contrast, goethite notably promoted the biofilm formation and there was less biofilm detected in montmorillonite containing system. The percentage of the survival bacteria in the biofilm that formed on montmorillonite, kaolinite and goethite was 53.8%, 40.8% and 28.2%. In addition, there were more reactive oxygen species (ROS) were detected in the cells that exposed to goethite than those of the cells exposed to kaolinite and montmorillonite. These results suggest that the electrostatic repulsion between kaolinite/montmorillonite and strain DNS10 prevents them from contacting each other and facilitates bacterial growth by allowing the strain to obtain more nutrients. Oppositely, the needle-like morphology of goethite might damage the strain DNS10 cell when they were combined by electrostatic attraction, and the goethite induced ROS also aggravate the cytotoxicity of goethite on strain DNS10. In addition, the relative transcription of trzN in the cells contacted with montmorillonite, kaolinite and goethite was 0.94-, 0.27- and 0.20- fold of the no mineral exposure treatment. Briefly, this research suggests that the minerals with different structure and/or physicochemical characteristics might cause various trend for the biofilm formation and degradation potential of the bacteria.

Topics: Arthrobacter; Atrazine; Bentonite; Biofilms; Iron Compounds; Kaolin; Minerals; Reactive Oxygen Species; Soil; Soil Pollutants

Topics: Adsorption; Anti-Bacterial Agents; Cations; Ferrosoferric Oxide; Iron; Kaolin; Minerals; Quinolones; Sulfonamides; Water

The increased applications and production of graphene oxide (GO) make the necessity to study information on the interaction of GO with minerals. In this work, adsorption and desorption were used to study the reversibility of interaction between GO and goethite/kaolinite. Result showed that the pH value, ionic strength, and temperature had significant effects on the adsorption and desorption behavior of GO. Interaction force was stronger between GO and goethite than that of kaolinite. The interaction may be attributed to the electrostatic, hydrogen-bonding, and Lewis acid base interactions. The irreversible interaction between GO and minerals may be a main mechanism for the observed desorption hysteresis. These results are important for evaluating the fate and health risk of GO in the environment.

Topics: Adsorption; Graphite; Hydrogen-Ion Concentration; Iron Compounds; Kaolin; Minerals; Osmolar Concentration; Temperature

The effects of low-molecular-weight organic acids (LMWOAs) on the transport of graphene oxide nanoparticles in saturated kaolinite- and goethite-coated sand columns were studied. Acetic acid, glycolic acid, malonic acid, and tartaric acid were chosen in the experiments. LMWOAs enhanced the mobility of GO by electrostatic/steric repulsion. In addition, they competed with GO for limited deposition sites on grain surfaces. The effects of organic acids on the transport of GO strongly depended on organic acid species. In general, the transport enhancement effects followed the order of tartaric acid > malonic acid > glycolic acid > acetic acid; this difference may be related to the number and type of functional groups of organic acids. Different LMWOAs enhanced the transport of GO in goethite-coated sand to a larger extent than did in kaolinite-coated sand under the test conditions; this was likely related to the differences of physicochemical characteristics between goethite and kaolinite. Organic acids significantly inhibited the deposition of GO at 0.5 mM Ca

Topics: Adsorption; Carboxylic Acids; Graphite; Iron Compounds; Kaolin; Minerals; Molecular Weight; Nanoparticles; Silicon Dioxide; Soil; Soil Pollutants; Static Electricity

This study evaluates different methods to determine points of zero charge (PZCs) on five organic materials, namely maple sawdust, wood ash, peat moss, compost, and brown algae, used for the passive treatment of contaminated neutral drainage effluents. The PZC provides important information about metal sorption mechanisms. Three methods were used: (1) the salt addition method, measuring the PZC; (2) the zeta potential method, measuring the isoelectric point (IEP); (3) the ion adsorption method, measuring the point of zero net charge (PZNC). Natural kaolinite and synthetic goethite were also tested with both the salt addition and the ion adsorption methods in order to validate experimental protocols. Results obtained from the salt addition method in 0.05 M NaNO

Topics: Adsorption; Green Chemistry Technology; Iron Compounds; Isoelectric Point; Kaolin; Metals; Minerals; Waste Disposal, Fluid

Soil, composed mainly of minerals, plays a central role in the circulation of microbial pathogens in the environment. Herein, the growth, biofilm formation, and virulence gene expression of the pathogenic bacteria Escherichia coli O157:H7 were monitored following exposure to montmorillonite, kaolinite, and goethite, three common soil minerals in the clay size fraction. E. coli O157:H7 growth was notably promoted (P < 0.05), while biofilm formation was inhibited in the presence of montmorillonite (P < 0.05), which is attributed to the suppression of colanic acid (CA) production and an increase in bacterial motility. Kaolinite not only promoted bacterial growth (P < 0.05), but also contributed to biofilm formation upon stimulating CA production. Upon exposure to goethite, notably slower bacterial growth and higher biomass of biofilm were observed as compared to the control (P < 0.05). Goethite stimulated the synthesis of CA to encase cells in a protective biofilm in response to the tight association between bacteria and goethite, which could cause bacterial death. Additionally, the transcription of virulence factors (stxA-1 and stxA-2) was significantly decreased in goethite or kaolinite system (P < 0.05). These findings indicate that minerals play important roles in the physiological state of bacteria and ultimately govern the fate of this pathogen in soils.

Topics: Bentonite; Biofilms; Clay; Escherichia coli O157; Iron Compounds; Kaolin; Minerals; Soil; Virulence

The Talbragar Fish Bed is one of Australia's most important Jurassic deposits for freshwater fishes, land plants and aquatic and terrestrial insects. The site has yielded many well preserved fossils, which has led to the formal description of numerous new species and higher taxa. The excellent preservation of many fossils has allowed detailed anatomical studies, e.g. of the early teleost fish Cavenderichthys talbragarensis (Woodward, 1895). Here we report on the fluorescent characteristics and mineral composition of a range of Talbragar fossils. Most specimens fluoresce under ultraviolet, blue and green light. Elemental and mineralogical analyses revealed that the Talbragar fossils consist predominantly of quartz (SiO2), a mineral that is likely to account for the observed fluorescence, with trace kaolinite (Al2Si2O5(OH)4) in some of the fish fossils. Rock matrices are predominantly composed of quartz and goethite (FeO(OH)). Closer inspection of a plant leaf (Pentoxylon australicum White, 1981) establishes fluorescence as a useful tool for the visualisation of anatomical details that are difficult to see under normal light conditions.

Topics: Animals; Australia; Biological Evolution; Fishes; Fossils; History, Ancient; Insecta; Iron Compounds; Kaolin; Luminescent Measurements; Metals, Heavy; Minerals; Plant Leaves; Plants; Quartz; Spectrometry, Fluorescence

The pesticide gibberellic acid (GA

Topics: Adsorption; Bentonite; Diffusion; Endocrine Disruptors; Ferric Compounds; Gibberellins; Iron Compounds; Kaolin; Kinetics; Minerals

The adsorption of extracellular polymeric substances (EPS) from Pseudomonas putida on montmorillonite, kaolinite and goethite was investigated as a function of pH using batch studies coupled with confocal laser scanning microscopy (CLSM) and isothermal titration calorimetry (ITC). Characterization by Raman spectroscopy, X-ray photoelectron spectroscopy (XPS) and Fourier transform infrared (FTIR) spectroscopy showed that the extracted EPS contained carboxyl, phosphoryl, amino, and hydroxyl on functional groups as well as polysaccharides, protein and nucleic acid on components. The mass fraction of EPS adsorption on minerals decreased with the final pH increased from 3.0 to 9.0. The mass fraction of EPS-N adsorption varied with pH values and was higher than that of EPS-C or EPS-P on montmorillonite and kaolinite, while the mass fraction of EPS-P adsorption was the highest on goethite. CLSM results further demonstrated that proteins were predominantly distributed on the montmorillonite and kaolinite surfaces, while nucleic acids were mainly on the goethite surface. ITC results revealed that the adsorption process in all mineral systems was exothermic, and pH altered the heat effect of EPS-mineral reactions. The data obtained in this study would facilitate a better understanding of the adsorption mechanisms of EPS on minerals.

Topics: Adsorption; Algorithms; Bacterial Proteins; Bentonite; Calorimetry; DNA, Bacterial; Extracellular Space; Hydrogen-Ion Concentration; Iron Compounds; Kaolin; Microscopy, Confocal; Minerals; Photoelectron Spectroscopy; Polymers; Polysaccharides; Pseudomonas putida; RNA, Bacterial; Soil; Spectroscopy, Fourier Transform Infrared; Surface Properties

Isoflavones are compounds whose presence in the aquatic environment is increasingly recognized and may be of concern due to their potential to act as endocrine disruptors. Sorption to particles may be a relevant removal mechanism for isoflavones. This work investigated the influence of pH, ionic strength, and sediment composition on sorption of genistein and daidzein, two key isoflavones, using sorption isotherms and edges. The effect of sorbed isoflavones on the survival, growth, and predator avoidance performance of larval fathead minnows (Pimephales promelas) was assessed. Sorption to goethite and kaolinite was pH-dependent, with a maximum near pH 7 for both compounds. Sorption to montmorillonite was ionic-strength dependent but largely pH-independent. Overall, sorption to sediments is likely to sequester less than 5% of isoflavones in a discharge. No statistically significant effects were observed for larvae exposed to sorbed isoflavones, suggesting that sorption to sediments reduces exposure to isoflavones.

Topics: Adsorption; Animals; Bentonite; Cyprinidae; Escape Reaction; Genistein; Geologic Sediments; Hydrogen-Ion Concentration; Iron Compounds; Isoflavones; Kaolin; Larva; Minerals; Osmolar Concentration; Rivers; Water Pollutants, Chemical

Upon release into waters, sediments, and soils, graphene oxide (GO) may interact with fine mineral particles. We investigated the heteroaggregation of GO with different minerals, including montmorillonite, kaolinite, and goethite, in aqueous phase. GO significantly enhanced the dispersion of positively charged goethite (>50%) via heteroaggregation, while there was no interaction between GO and negatively charged montmorillonite or kaolinite. Electrostatic attraction was the dominant force in the GO-goethite heteroaggregation (pH 4.0-8.5), and the dissolved Fe ions (<0.16 mg/L) from goethite were unable to destabilize GO suspension. The GO-goethite heteroaggregation was further quantitatively investigated through GO adsorption study. All adsorption isotherms of GO at different solution pH (4.0 and 6.5) followed the Linear model. The apparent intercept (1.0-6.9 mg/g) was observed for all the adsorption isotherms, indicating that this fraction of adsorbed GO was difficult to desorb from goethite (defined here as irreversible adsorption) under the tested conditions. Desorption hysteresis was observed, which could be explained by the formation of multilayered GO-goethite complex with high configurational stability. These findings are useful for understanding the interaction of GO with mineral surfaces, and potential fate and toxicity of GO under natural conditions in aquatic environments, as well as in soils and sediments.

Topics: Adsorption; Bentonite; Graphite; Iron Compounds; Kaolin; Minerals; Soil; Suspensions; Water

Oxidation of Cr(III) by manganese oxides may pose a potential threat to environments due to the formation of toxic Cr(VI) species. At present, it was still unclear whether the extent of Cr(III) oxidation and fate of Cr(VI) would be changed when manganese oxides co-exist with other minerals, the case commonly occurring in soils. This study investigated the influence of goethite and kaolinite on Cr(III) oxidation by birnessite under acidic pH condition (pH3.5) and background electrolyte of 0.01mol/L NaCl. Goethite was found not to affect Cr(III) oxidation, which was interpreted as the result of overwhelming adsorption of cationic Cr(III) onto the negatively-charged birnessite (point of zero charge (PZC)<3.0) rather than the positively-charged goethite (PZC=8.8). However, more Cr(VI) would be retained by the surface with the increase in addition of goethite because of its strong ability on adsorption of Cr(VI) at low pH. Moreover, either Cr(III) oxidation or distribution of the generated Cr(VI) between the solid and solution phases was not affected by kaolinite (PZC<3.0), indicating its low affinity for Cr species. Reactions occurring in the present mixed systems were suggested, which could be partly representative of those in the soils and further indicates that the mobility and risk of Cr(VI) would be decreased if goethite was present.

Topics: Chromium; Hydrogen-Ion Concentration; Iron Compounds; Kaolin; Minerals; Oxidation-Reduction; Oxides; Surface Properties

In the present study, the influence of kaolinite and goethite on microbial degradation of methyl parathion was investigated. We observed that the biodegradation process was improved by kaolinite and depressed by goethite. Calorimetric data further showed that the metabolic activities of degrading cells (Pseudomonas putida) were enhanced by the presence of kaolinite and depressed by the presence of goethite. A semipermeable membrane experiment was performed and results supported the above observations: the promotive effect of kaolinite and the inhibition of goethite for microbial degradation was not found when the bacteria was enclosed by semipermeable membrane and had no direct contact with these minerals, suggesting the important function of the contact of cellular surfaces with mineral particles. The relative larger particles of kaolinite were loosely attached to the bacteria. This attachment made the cells easy to use the sorbed substrate and then stimulated biodegradation. For goethite, small particles were tightly bound to bacterial cells and limited the acquisition of substrate and nutrients, thereby inhibiting biodegradation. These results indicated that interfacial interaction between bacterial cells and minerals significantly affected the biodegradation of pesticides.

Topics: Adsorption; Biodegradation, Environmental; Biological Transport; Insecticides; Iron Compounds; Kaolin; Kinetics; Membranes, Artificial; Methyl Parathion; Minerals; Particle Size; Permeability; Pseudomonas putida; Thermodynamics

Many aquifers contaminated by U(VI)-containing acidic plumes are composed predominantly of quartz-sand sediments. The F-Area of the Savannah River Site (SRS) in South Carolina (USA) is an example. To predict U(VI) mobility and natural attenuation, we conducted U(VI) adsorption experiments using the F-Area plume sediments and reference quartz, goethite, and kaolinite. The sediments are composed of ∼96% quartz-sand and 3-4% fine fractions of kaolinite and goethite. We developed a new humic acid adsorption method for determining the relative surface area abundances of goethite and kaolinite in the fine fractions. This method is expected to be applicable to many other binary mineral pairs, and allows successful application of the component additivity (CA) approach based surface complexation modeling (SCM) at the SRS F-Area and other similar aquifers. Our experimental results indicate that quartz has stronger U(VI) adsorption ability per unit surface area than goethite and kaolinite at pH ≤ 4.0. Our modeling results indicate that the binary (goethite/kaolinite) CA-SCM under-predicts U(VI) adsorption to the quartz-sand dominated sediments at pH ≤ 4.0. The new ternary (quartz/goethite/kaolinite) CA-SCM provides excellent predictions. The contributions of quartz-sand, kaolinite, and goethite to U(VI) adsorption and the potential influences of dissolved Al, Si, and Fe are also discussed.

Topics: Adsorption; Geologic Sediments; Humic Substances; Iron Compounds; Kaolin; Kinetics; Minerals; Models, Theoretical; Quartz; Silicon Dioxide; Soil Pollutants, Radioactive; South Carolina; Surface Properties; Temperature; Uranium; Water Pollutants, Radioactive

The mobility of an acidic uranium waste plume in the F-Area of Savannah River Site is of great concern. In order to understand and predict uranium mobility, U(VI) adsorption experiments were performed as a function of pH using background F-Area aquifer sediments and reference goethite and kaolinite (major reactive phases of F-Area sediments), and a component-additivity (CA) based surface complexation model (SCM) was developed. Our experimental results indicate that the fine fractions (≤45 μm) in sediments control U(VI) adsorption due to their large surface area, although the quartz sands show a stronger adsorption ability per unit surface area than the fine fractions at pH < 5.0. Kaolinite is a more important sorbent for U(VI) at pH < 4.0, while goethite plays a major role at pH > 4.0. Our CA model combines an existing U(VI) SCM for goethite and a modified U(VI) SCM for kaolinite along with estimated relative surface area abundances of these component minerals. The modeling approach successfully predicts U(VI) adsorption behavior by the background F-Area sediments. The model suggests that exchange sites on kaolinite dominate U(VI) adsorption at pH < 4.0, goethite and kaolinite edge sites cocontribute to U(VI) adsorption at pH 4.0-6.0, and goethite dominates U(VI) adsorption at pH > 6.0.

Topics: Adsorption; Geologic Sediments; Georgia; Groundwater; Hydrogen-Ion Concentration; Iron Compounds; Kaolin; Minerals; Models, Chemical; Quartz; Radioactive Pollutants; Uranium

The adsorption of extracellular polymeric substances (EPS) from Bacillus subtilis on montmorillonite, kaolinite and goethite was investigated as a function of pH and ionic strength using batch studies coupled with Fourier transform infrared (FTIR) spectroscopy. The adsorption isotherms of EPS on minerals conformed to the Langmuir equation. The amount of EPS-C and -N adsorbed followed the sequence of montmorillonite>goethite>kaolinite. However, EPS-P adsorption was in the order of goethite>montmorillonite>kaolinite. A marked decrease in the mass fraction of EPS adsorption on minerals was observed with the increase of final pH from 3.1 to 8.3. Calcium ion was more efficient than sodium ion in promoting EPS adsorption on minerals. At various pH values and ionic strength, the mass fraction of EPS-N was higher than those of EPS-C and -P on montmorillonite and kaolinite, while the mass fraction of EPS-P was the highest on goethite. These results suggest that proteinaceous constituents were adsorbed preferentially on montmorillonite and kaolinite, and phosphorylated macromolecules were absorbed preferentially on goethite. Adsorption of EPS on clay minerals resulted in obvious shifts of infrared absorption bands of adsorbed water molecules, showing the importance of hydrogen bonding in EPS adsorption. The highest K values in equilibrium adsorption and FTIR are consistent with ligand exchange of EPS phosphate groups for goethite surface. The information obtained is of fundamental significance for understanding interfacial reactions between microorganisms and minerals.

Topics: Adsorption; Aluminum Silicates; Bacillus subtilis; Bentonite; Biopolymers; Carbon; Clay; Extracellular Space; Ferric Compounds; Hydrogen-Ion Concentration; Iron Compounds; Kaolin; Minerals; Nitrogen; Osmolar Concentration; Phosphorus; Spectroscopy, Fourier Transform Infrared; Temperature

In this investigation, Raman spectroscopy with 1064 and 632.8 nm excitation was used to investigate real mineral samples of bauxite ore from mines of Northern Brazil, together with Raman mapping and X-rays diffraction. The obtained results show clearly that the use of microRaman spectroscopy is a powerful tool for the identification of all the minerals usually found in bauxites: gibbsite, kaolinite, goethite, hematite, anatase and quartz. Bulk samples can also be analysed, and FT-Raman is more adequate due to better signal-to-noise ratio and representativity, although not efficient for kaolinite. The identification of fingerprinting vibrations for all the minerals allows the acquisition of Raman-based chemical maps, potentially powerful tools for process mineralogy applied to bauxite ores.

Topics: Aluminum Oxide; Brazil; Ferric Compounds; Iron Compounds; Kaolin; Minerals; Quartz; Spectrum Analysis, Raman; Titanium; X-Ray Diffraction

To ensure safe and efficient geologic CO(2) sequestration (GCS), it is crucial to have a better understanding of CO(2)-brine-rock interactions under GCS conditions. In this work, using biotite (K(Mg,Fe)(3)AlSi(3)O(10)(OH,F)(2)) as a model clay mineral, brine-biotite interactions were studied under conditions relevant to GCS sites (95 °C, 102 atm CO(2), and 1 M NaCl solution). After reaction for 3-17 h, fast growth of fibrous illite on flat basal planes of biotite was observed. After 22-70 h reaction, the biotite basal surface cracked, resulting in illite detaching from the surface. Later on (96-120 h), the cracked surface layer was released into solution, thus the inner layer was exposed as a renewed flat basal surface. The cracking and detachment of the biotite surface layer increased the surface area in contact with solution and accelerated biotite dissolution. On biotite edge surfaces, Al-substituted goethite and kaolinite precipitated. In control experiments with water under the same temperature and pressure, neither macroscopic fibrous illite nor cracks were observed. This work provides unique information on biotite-brine interaction under acidic hydrothermal conditions.

Topics: Aluminum Silicates; Carbon Sequestration; Ferrous Compounds; Hydrogen-Ion Concentration; Iron Compounds; Kaolin; Minerals; Pressure; Seawater; Spectrometry, X-Ray Emission; Surface Properties; Temperature

The basic properties of goethite, kaolinite and their association were characterized using X-ray diffraction (XRD) , scanning electron microscopes (SEM), Fourier transform infrared spectroscopy (FT-IR), potentiometric titrations, specific surface area (SSA) and micropore analysis. Moreover, the adsorption capacity and adsorption models of fluoride by the investigated samples were studied. Results show that when kaolinite and goethite presented simultaneously in the same suspension system, goethite was apt to coat the surface of kaolinite and the interactions between them could occur rapidly. As a result, the binary association containing kaolinite and goethite was formed. The binary association possessed the pore diameter of 0.42 nm and 0.61 nm, specific surface area of 34.08 m2/g, surface fractal dimension of D = 2.726 and the pH(PZNPC) (pH of point of zero net proton charge) in the range of 5.50-6.50. At the initial pH 6. 00, the maximum adsorption capacity (q(max) of goethite, kaolinite and association was 4.506, 0.608 and 3.520 mg/g respectively. The adsorption of fluoride by the single kaolinite or goethite could be attributed to monolayer adsorption and the data of isotherm adsorption could be well fitted by Langmuir model (R2 = 0.991 and R2 = 0.964 respectively). The Freundlich model was suitable for describing the adsorption of fluoride by the binary association (R2 = 0.995), which indicated that the surface of the binary association is heterogeneous and is probably provided with multilayer adsorption sites. The adsorption mechanisms for fluoride by the investigated samples include anion ligand exchange, surface coordination and electrostatic attraction. In addition, F acting as a bond bridge between the surfaces of kaolinite and goethite contributed to the adsorption of fluoride too. Compared to the single goethite or kaolinite, the binary association exhibited the higher specific surface area, surface fractal dimension and adsorption capacity for fluoride as well as the lower amount of hydroxyls and net proton charges on it's surface, although no significant variation was found in the porosity structure of the association.

Topics: Adsorption; Environmental Pollutants; Fluorides; Iron Compounds; Kaolin; Minerals; Models, Chemical; Surface Properties

Adsorption and desorption of salmon sperm DNA on bacteria (Bacillus thuringiensis, Pseudomonas putida), two different colloidal fractions (organic and inorganic clay) from an Alfisol, minerals (montmorillonite, kaolinite and goethite) and colloid-bacteria composites were studied. Similar adsorption capacity and affinity of DNA were observed on two bacterial cells. However, the two bacterial strains played different roles in affecting the adsorption of DNA on the composites of soil colloidal particles with bacteria. The introduction of B. thuringiensis in soil colloids and minerals systems dramatically promoted DNA adsorption on colloidal particles especially organic clay, while P. putida decreased the adsorption of DNA on kaolinite and goethite. Electrostatic force and ligand exchange are regarded to be the major driving forces involved in the adsorption of DNA on bacterial cells, montmorillonite, soil colloids and goethite. Presence of bacteria enhanced the proportion of DNA adsorption on soil colloidal particles by electrostatic force and depressed that by ligand exchange process. Information obtained in this study is of fundamental significance for the understanding of the ultimate fate of extracellular DNA in soil systems.

Topics: Adsorption; Animals; Bacillus thuringiensis; Bentonite; Colloids; DNA; Hydrogen-Ion Concentration; Iron Compounds; Kaolin; Male; Minerals; Phosphates; Pseudomonas putida; Salmon; Sodium Chloride; Soil; Temperature

This paper studied the characteristics of the adsorption and desorption of Bt (Bacillus thuringiensis) toxin on goethite, kaolinite, and silica. The results showed that in phosphate buffer (pH 8), the adsorption isotherms of Bt toxin on the test minerals followed Langmuir equation (R2 >0. 9661), and the adsorbed amounts were in the order of goethite > kaolinite > silica. The Bt toxin was easily adsorbed on the minerals, and the adsorption could reach equilibrium after 1 hour. Within the range of pH 6-8, the amounts of Bt toxin adsorbed on goethite, kaolinite and silica decreased with increasing pH; in the range of 10 degrees C-50 degrees C, the amounts of the toxin adsorbed on goethite and silica decreased by 8.39% and 47.06%, respectively, while that on kaolinite increased slightly (5.91%). The infrared absorption spectrum showed that there was only a minor alteration of Bt toxin after adsorption. The toxin adsorbed on the minerals was not easily desorbed by deionised water, with the desorption rate ranged from 28.48% to 42.04% after three times washing.

Topics: Adsorption; Bacillus thuringiensis; Bacillus thuringiensis Toxins; Bacterial Proteins; Bacterial Toxins; Endotoxins; Hemolysin Proteins; Hydrogen-Ion Concentration; Iron Compounds; Kaolin; Kinetics; Minerals; Silicon Dioxide; Spectrophotometry, Infrared

Ciprofloxacin (CIP)-soil sorption interactions by surface complexation (via -COOH group) and cation exchange (-NH3+ group) were estimated by use of the structurally related probe compounds flumequine (FQ) (-COOH) and phenylpiperazine (PP) (-NH3+). Comparison of CIP and FQ sorption by surface complexation on goethite indicated a 0.7 times lower driving force for sorption, K(xs), for CIP than for FQ, with a model that assumed functional group interactions were enhanced by the hydrophobicity of the rest of the molecule. Similarly, K(xs) was 9.5 times greater for CIP than for PP for sorption by cation exchange on kaolinite and montmorillonite. Use of the pure phase sorbent K(xs) scaling factors between PP, FQ, and CIP for eight soils with a range of clay and oxide contents yielded total sorbed CIP concentrations that were within a factor of 2 (at pH 7.2) or less (at pH 5) of observed values. The estimated relative contributions of CIP cation-exchange versus complexation interactions increased for soils with increasing cation-exchange capacity. The agreement between independently estimated and observed CIP sorption indicates that the use of probe compounds has the potential to provide quantitative measures of sorption contributions for other complex sorbates with multiple functional groups, including other emerging contaminants and pesticides.

Topics: Anti-Infective Agents; Cations; Ciprofloxacin; Iron Compounds; Kaolin; Minerals; Molecular Probes; Molecular Structure; Soil; Soil Pollutants

Adsorption of Pseudomonas putida on minerals including montmorillonite, kaolinite and goethite was studied. The adsorption isotherms of P. putida on the examined minerals conformed to the Langmuir equation. The amount of P. putida adsorbed followed the order: goethite > kaolinite > montmorillonite. A greater extent of P. putida adsorption on minerals was observed in the range of temperature from 15 to 35 degrees C. The adsorption of P. putida on minerals decreased with the increase of pH from 3.0 to 10.0. Magnesium ion was more efficient than sodium ion in promoting P. putida adsorption on minerals. The results suggest that electrostatic interactions play a vital role in P. putida adsorption by soil colloidal factions. The information obtained in this study is of fundamental significance for the understanding of the survival and transport of bacteria in soil systems.

Topics: Adsorption; Aluminum Silicates; Bacterial Proteins; Bentonite; Clay; Ferric Compounds; Iron Compounds; Kaolin; Minerals; Pseudomonas putida

Polymerase chain reaction (PCR) was used to amplify a 600-base pair (bp) sequence of plasmid pGEX-2T DNA bound on soil colloidal particles from Brown soil (Alfisol) and Red soil (Ultisol), and three different minerals (goethite, kaolinite, montmorillonite). DNA bound on soil colloids, kaolinite, and montmorillonite was not amplified when the complexes were used directly but amplification occurred when the soil colloid or kaolinite-DNA complex was diluted, 10- and 20-fold. The montmorillonite-DNA complex required at least 100-fold dilution before amplification could be detected. DNA bound on goethite was amplified irrespective of whether the complex was used directly, or diluted 10- and 20-fold. The amplification of mineral-bound plasmid DNA by PCR is, therefore, markedly influenced by the type and concentration of minerals used. This information is of fundamental importance to soil molecular microbial ecology with particular reference to monitoring the fate of genetically engineered microorganisms and their recombinant DNA in soil environments.

Topics: Aluminum Silicates; Animals; Bentonite; Cattle; Clay; Colloids; DNA, Bacterial; Iron Compounds; Kaolin; Minerals; Plasmids; Polymerase Chain Reaction; Soil

This study investigated the transformation of carbon tetrachloride (CT) by goethite, hematite, magnetite, and kaolinite treated with bisulfide to form coatings of iron monosulfide (FeS) and other Fe(II) species. These coatings contribute to abiotic natural attenuation in anaerobic environments. Batch kinetic experiments were performed under anoxic conditions at pH 8.0. Surface-area-normalized pseudo-first-order rate constants for CT transformation did not differ significantly for the three HS- treated iron oxides, but the rate of CT transformation by bisulfide-treated kaolinite was significantly lower, most likely due to kaolinite's lower iron content. The yield of chloroform (CF) from CT transformation was typically approximately 1%. There was negligible or only slight adsorption of several natural organic matter (NOM) model compounds to the surface of HS- treated goethite, and these compounds had no influence on CT transformation rate constants or CF yields. Juglone, on the other hand, adsorbed to a greater extent, and also significantly influenced the CF yield, increasing it by a factor of approximately 20 for HS- treated hematite. We speculate that juglone or its HS- addition product adsorbed to the mineral surface and acted as a hydrogen atom donor that reacted with the trichloromethyl radical intermediate, increasing the CF yield.

Topics: Adsorption; Carbon Tetrachloride; Carboxylic Acids; Catechols; Chloroform; Ferric Compounds; Ferrosoferric Oxide; Hydroquinones; Hydroxybenzoates; Iron Compounds; Kaolin; Minerals; Naphthoquinones; Oxidation-Reduction; Sulfides; Water Pollutants, Chemical

Adsorption, desorption and activity of acid phosphatase on various soil colloidal particles and pure clay minerals were studied. Higher adsorption amounts and low percentage of desorption of acid phosphatase were found on fine soil clays (<0.2 microm). Electrostatic force and ligand exchange are the major driving forces that are involved in the adsorption of enzymes on soil clays. More enzyme molecules were adsorbed on soil clays in the presence of organic components. However, enzymes on organic clays were more easily released. One-third of the enzyme on goethite was adsorbed via ligand exchange process. Some other interactions, such as van der Waals force, hydrophobic force and hydrogen bonding may be more important in the adsorption of enzyme on kaolinite and the enzyme in this system cannot be easily removed. Coarse clays (0.2-2 microm) and inorganic soil clays had higher affinities for enzyme molecules than fine clays and organic clays, respectively. The activity of enzyme bound on soil clays was inhibited and the thermal stability was increased in the presence of organic matter. Data obtained in this study are helpful for a better understanding of the interactions of enzymes with inorganic and organic constituents in soil and associated environments.

Topics: Acid Phosphatase; Adsorption; Aluminum Silicates; Clay; Colloids; Hydrogen-Ion Concentration; Iron Compounds; Kaolin; Ligands; Minerals; Particle Size; Sensitivity and Specificity; Soil; Surface Properties; Temperature

The present work investigates the adsorption and mobility (desorption) of As(III) and As(V) on an oxisol, and its main mineral constituents, as part of a broader project aimed at selecting a soil liner to be used in tailings dams at a sulfidic gold ore plant. Emphasis was given to a quantitative comparison of As mobility-here assessed by the amount of As leached from the loaded samples-under different experimental conditions. From among the soil constituents, goethite was the most efficient adsorbent with regard to arsenic adsorption, 12.4 mg x g(-1) for As(V) and 7.5 mg x g(-1) for As(III), respectively. Gibbsite also presented a relevant adsorption capacity (4.6 mg x g(-1) for As(V) and 3.3 mg x g(-1) for As(III)); adsorption on kaolinite was negligible (<0.23 mg x g(-1) for As(V) and As(III)). Desorption of the arsenic was shown to vary largely with the arsenic oxidation state, the adsorbents and the leaching solutions. While only 1-2% max. of As(V) was released from the loaded samples, leaching the A(III) reached 32%, the highest values corresponding to the solutions containing sulfate ions. Oxisol and goethite were superior to gibbsite with respect to As immobilization. Adsorption and mobility were also discussed with the help of electrophoretic mobility and isoelectric points (IEP) determined prior and following arsenic adsorption on goethite and gibbsite. The results indicated that As(V) is mainly adsorbed as an inner sphere complex. As(III) may be adsorbed as an inner or an outer neutral complex.

Topics: Adsorption; Arsenic; Brazil; Electrophoretic Mobility Shift Assay; Geologic Sediments; Gold; Hydrogen-Ion Concentration; Iron Compounds; Isoelectric Point; Kaolin; Minerals; Mining; Oxides; Soil Pollutants; Sulfides

Adsorption of acid phosphatase on goethite, kaolinite and two colloids from the soils in central and south China in the presence of organic acids and phosphate was studied. With the increase of anion concentration, the ability in decreasing enzyme adsorption followed the sequence: phosphate>tartrate>oxalate>acetate. Acetate showed promotive effect on enzyme adsorption at lower anion concentrations whereas oxalate, tartrate and phosphate compete effectively with enzyme in a broad range of anion concentration. The adsorption isotherms of enzyme in most of the anionic systems studied conformed to the Langmuir equation. Phosphate reduced the affinity of enzyme on goethite more significantly than the other anions. However, tartrate decreased the affinity of enzyme on soil colloids and kaolinite to a greater extent than phosphate, oxalate and acetate. This observation suggested that the impact of anions on enzyme adsorption varies with anionic type and the surface characteristics of soil components. The influence of the addition order of ligand on enzyme adsorption was found greater in tartrate and phosphate systems. In general, simultaneous introduction of ligand and enzyme into the system had the lowest enzyme adsorption, showing more competition between ligand and enzyme molecules in this system. Data from this work indicated that the status and activity of enzyme in certain soil microenvironments especially the rhizosphere where various organic and inorganic ligands are active can be altered and may be completely different from the bulk soil.

Topics: Acid Phosphatase; Acids, Acyclic; Adsorption; Colloids; Iron Compounds; Kaolin; Minerals; Phosphates; Soil

Sorption of the endocrine-disrupting chemical 17beta-estradiol (E(2)) from aqueous solutions to goethite, an iron oxide, and the clay minerals kaolinite, illite, and montmorillonite (K and Ca forms) was measured at 25 degrees C. The clay minerals sorbed more E(2) than the oxide, with sorption capacity increasing in the order goethite

Topics: Adsorption; Bentonite; Estradiol; Iron Compounds; Kaolin; Minerals; Soil